%% filename: amsart-template.tex %% American Mathematical Society %% AMS-LaTeX v.2 template for use with amsart %% ==================================================================== \documentclass{amsart} \usepackage{amssymb} \usepackage{graphicx} \usepackage{tikz} \usetikzlibrary{backgrounds} \newtheorem{theorem}{Theorem}[section] \newtheorem{lemma}[theorem]{Lemma} \newtheorem{corollary}[theorem]{Corollary} \newtheorem{proposition}[theorem]{Proposition} \newtheorem{conjecture}[theorem]{Conjecture} \theoremstyle{definition} \newtheorem{definition}[theorem]{Definition} \newtheorem{example}[theorem]{Example} \newtheorem{xca}[theorem]{Exercise} \theoremstyle{remark} \newtheorem{remark}[theorem]{Remark} \numberwithin{equation}{section} \begin{document} \title{Nested Tire Decompositions of Plane Triangulations} % author one information \author{Eric Bauerfeld} \address{} \curraddr{} \email{} \thanks{} \subjclass[2010]{Primary } \keywords{plane graph, triangulation, plane depth, level edge, dual graph, tire graph} \date{} \dedicatory{} \begin{abstract} We establish the foundational structure of nested level-induced tire decompositions of a plane triangulation $G$. A \emph{level source} of $G$ induces a BFS layering of $G$ and endows the inner planar dual $G'$ with a \emph{dual depth} grading. The basic object of study is the \emph{tire graph} $T$ --- a plane graph whose outer and inner boundaries bound a closed planar region, the \emph{tire tread} $R$, triangulated by the \emph{annular edges} $E_{\mathrm{ann}}$. We define medial tire graphs and prove a basic colour-count bound for their annular medial cycle. Our main structural results are the \emph{tire-component lemma}, the \emph{tire-tread partition theorem}, and the rooted \emph{tire-tree decomposition}, which together organize the bounded faces of $G$ into nested tire treads. \end{abstract} \maketitle \section{Introduction} A classical theorem of Tait recasts the Four Colour Theorem in dual, edge-colouring terms: a plane triangulation $G$ is properly $4$-vertex-colourable if and only if its dual cubic graph $G'$ is properly $3$-edge-colourable. Thus a minimal counterexample to the Four Colour Theorem -- a smallest triangulation admitting no proper $4$-colouring -- corresponds to a smallest cubic plane graph admitting no proper $3$-edge-colouring. The structural study of such a minimal counterexample is the overarching motivation for the present line of work. This first paper establishes the foundational vocabulary --- level sources, dual depth, tire graphs, and partial tire duals --- on which subsequent papers in the series build. In particular, the companion paper \cite{bauerfeld-nested-tire-duals} uses these definitions to develop nested-cycle structure theorems and chain-pigeonhole conjectures for tire annular subgraphs of $G'$. \paragraph{Related work.} The structural object underlying this programme --- the set of proper $4$-colourings of a boundary cycle that extend to a colouring of a bounded planar region --- is classical. Birkhoff's reducibility analysis of the diamond configuration~\cite{birkhoff-reducibility} is the earliest instance of computing such extension sets to attack the Four Colour Theorem; the chromatic polynomial framework of Birkhoff and Lewis~\cite{birkhoff-lewis-chromatic} systematised the counting. Tutte studied how the chromatic polynomial of a rooted planar triangulation decomposes along its outer boundary~\cite{tutte-chromatic-sums-1973} and developed an algebraic theory of graph colourings organised around separating subgraphs~\cite{tutte-algebraic-colorings, tutte-four-colour-conjecture}. The most recent and structurally closest parallel is Dvo\v{r}\'ak and Lidick\'y's analysis of \emph{coloring count cones}~\cite{dvorak-lidicky-cones}, which characterises the possible boundary-extension functions on a fixed outer cycle of a near-triangulation. The Heesch--Appel--Haken approach~\cite{heesch-untersuchungen, robertson-sanders-seymour-thomas} also uses boundary-extension reasoning, but case-by-case on a finite unavoidable set of local configurations rather than as part of a global structural induction. The tire-tree decomposition introduced here differs from each of these in shape rather than ingredients. Birkhoff, Tutte, and Dvo\v{r}\'ak--Lidick\'y all study \emph{one} boundary; Heesch and the cleaned-up Appel--Haken proof~\cite{robertson-sanders-seymour-thomas} study a finite collection of local boundaries. The present framework organises the entire triangulation into a hierarchy of annular regions glued along level cycles, and asks whether boundary-extension constraints compose compatibly up the hierarchy. To the authors' knowledge, no prior work on the Four Colour Theorem has been organised around a global nested-cycle decomposition of this kind. Throughout, $G = (V, E)$ is a plane maximal planar graph (a triangulation) with a fixed planar embedding $\Pi_G$. We write $|V| = n$, so $|E| = 3n - 6$ and $G$ has $2n - 4$ triangular faces. \begin{definition}[Level source] A \emph{level source} of $G$ is a set $S \subseteq V$ that is either \begin{itemize} \item a single vertex $\{v\}$ (a \emph{vertex source}), or \item a set inducing a simple cycle in $G$ --- i.e.\ $G[S]$ is a simple cycle of length $\geq 3$ (a \emph{cycle source}). \end{itemize} \end{definition} \begin{definition}[Levels] Given a level source $S \subseteq V$, the \emph{level} of $v \in V$ is $\ell_G(v) = \mathrm{dist}_G(v, S)$, the graph distance from $v$ to the nearest source vertex. We write $L_d := \{v \in V : \ell_G(v) = d\}$ for the \emph{level-$d$ vertex set}, and abbreviate $L_{d}$, $L_{\leq d}$). \end{definition} \begin{definition}[Dual] \label{def:dual} The \emph{dual} of $G$, written $G'$, is the inner (weak) planar dual of $G$ with respect to the embedding $\Pi_G$: it has one vertex $d_f$ for each bounded face $f$ of $G$, and an edge joining $d_f$ and $d_{f'}$ for each edge of $G$ shared by two bounded faces $f$ and $f'$. The unbounded outer face contributes no vertex, and edges of $G$ on the outer boundary contribute no dual edge. Since $G$ is a triangulation, each vertex $d_f \in V(G')$ corresponds to a triangular face $f$ of $G$, and we write $V(f) \subseteq V$ for its three incident vertices. \end{definition} \begin{definition}[Dual depth] \label{def:dual-depth} Given a level source $S \subseteq V$, the \emph{dual depth} of a dual vertex $d_f \in V(G')$ is \[ \delta_G(d_f) = \min_{v \in V(f)} \ell_G(v) = \min_{v \in V(f)} \mathrm{dist}_G(v, S), \] the smallest level among the three vertices of $G$ bounding the face $f$. \end{definition} \begin{figure}[h] \centering \includegraphics[width=0.7\textwidth]{fig_dual_depth.png} \caption{Dual depth in a stacked-ring triangulation $G$ with level source $S = \{0\}$. Each $G$ vertex is labelled by its level $\ell$. Each bounded face carries a dual vertex (square, joined by dashed dual edges) coloured by its dual depth $\delta(d_f) = \min_{v \in V(f)} \ell(v)$: the central fan has depth $0$, the inner annulus depth $1$, and the outer annulus depth $2$. The outer face (the level-$3$ triangle) is excluded from the inner dual and carries no dual vertex.} \label{fig:dual-depth} \end{figure} \begin{definition}[Depth-$d$ dual subgraph and its components] \label{def:dual-component} For $d \geq 0$, the \emph{depth-$d$ dual subgraph} is \[ G'_d \;:=\; G'\bigl[\,\{d_f \in V(G') : \delta_G(d_f) = d\}\,\bigr], \] the inner-dual subgraph induced on the dual vertices of dual depth $d$. For a connected component $C'$ of $G'_d$ we write \[ F_{C'} := \{f : d_f \in V(C')\}, \qquad V_{C'} := \bigcup_{f \in F_{C'}} V(f), \] for its set of faces and the vertices of $G$ bounding them, and $R_{C'} := \bigcup_{f \in F_{C'}} f \subseteq |\Pi_G|$ for the closed planar region these faces cover. \end{definition} \begin{definition}[Tire graph] \label{def:tire-graph} A \emph{tire graph} consists of a plane graph $T$ together with an \emph{outer boundary} $B_{\mathrm{out}} \subseteq T$ and a \emph{connected inner outerplanar graph} $O \subseteq T$ with $V(B_{\mathrm{out}}) \cap V(O) = \emptyset$, where \begin{itemize} \item $B_{\mathrm{out}}$ is either a simple cycle of length $\geq 3$ or a single vertex (a \emph{degenerate outer boundary}); \item $O$ is a connected outerplanar graph; its \emph{inner boundary} $B_{\mathrm{in}}$ is the closed walk in $O$ that traces the boundary of $O$'s outer face in the inherited embedding, which is a simple cycle when $O$ is $2$-connected and a non-simple closed walk in general (visiting bridges twice and cut-vertices multiple times); if $|V(O)| = 1$, we say $T$ has a \emph{degenerate inner boundary}. \end{itemize} At most one of $B_{\mathrm{out}}, B_{\mathrm{in}}$ may be degenerate. The vertex and edge sets of $T$ are \[ V(T) = V(B_{\mathrm{out}}) \cup V(O), \qquad E(T) = E(B_{\mathrm{out}}) \cup E(O) \cup E_{\mathrm{ann}}, \] where $E_{\mathrm{ann}}$ --- the \emph{annular edges} --- has the property that, in the plane embedding of $T$, the closed planar region $R$ bounded externally by $B_{\mathrm{out}}$ and internally by $B_{\mathrm{in}}$ is partitioned into triangular faces of $T$ whose union is $R$. We call $R$ the \emph{tire tread} of $T$ and write $F_{\mathrm{ann}}$ for this set of triangular faces (the \emph{annular faces}). When $B_{\mathrm{out}}$ is a simple cycle and $O$ is $2$-connected, the tread is a closed annulus. More generally, $R$ is a closed planar region that may fail to be a $2$-manifold at cut-vertices of $O$ (where two ``lobes'' of the depth-$d$ region meet at a single vertex); the inner boundary $B_{\mathrm{in}}$ is then a non-simple closed walk that visits the cut-vertex multiple times. The relaxed definition accommodates outerplanar inner graphs with bridges or cut-vertices, while $O$ itself remains connected. When either boundary is degenerate, the tread is a closed disk with that vertex as apex. We summarize the data of a tire graph as the triple $T = (B_{\mathrm{out}}, O, E_{\mathrm{ann}})$, from which $B_{\mathrm{in}}$, the annular faces $F_{\mathrm{ann}}$, and the tread $R$ are determined; we freely identify a tire graph with its underlying plane graph $T$. \end{definition} \begin{figure}[h] \centering \includegraphics[width=0.78\textwidth]{fig_tire_example.png} \caption{A tire graph with non-degenerate boundaries: outer boundary $B_{\mathrm{out}}$ a $6$-cycle on vertices $0,\dots,5$ (blue), inner boundary $B_{\mathrm{in}}$ a $4$-cycle on vertices $6,\dots,9$ (red), inner outerplanar graph $O = B_{\mathrm{in}} \cup \{7\text{--}9\}$ (with one chord, orange), and $E_{\mathrm{ann}}$ (grey) tiling the annulus between $B_{\mathrm{out}}$ and $B_{\mathrm{in}}$ by ten triangular faces.} \label{fig:tire-example} \end{figure} \begin{definition}[Medial tire graph] \label{def:medial-tire-graph} Let $T = (B_{\mathrm{out}}, O, E_{\mathrm{ann}})$ be a tire graph. Let $T^{\circ}$ be the plane graph obtained from $T$ by deleting every edge of $O$ that is not on the inner boundary walk $B_{\mathrm{in}}$. Equivalently, $T^{\circ}$ keeps $B_{\mathrm{out}}$, $B_{\mathrm{in}}$, and the annular edges, but omits the chords of the inner outerplanar graph $O$. The \emph{medial tire graph} of $T$, denoted $M_{\mathrm{tire}}(T)$, is obtained from the medial graph $M(T^{\circ})$ by deleting every medial edge whose two endpoint-vertices correspond either to two edges of $B_{\mathrm{out}}$ or to two edges of $B_{\mathrm{in}}$. Thus $V(M_{\mathrm{tire}}(T))$ is naturally indexed by the non-chord edges of $T$, and two such vertices are adjacent exactly when the corresponding edges are consecutive on the boundary of a face of $T^{\circ}$, except for consecutive pairs lying wholly along one of the two boundary walks. The medial vertices corresponding to edges of $E_{\mathrm{ann}}$ are called the \emph{annular medial vertices}. \end{definition} \begin{figure}[h] \centering \includegraphics[width=0.78\textwidth]{fig_medial_tire_example.png} \caption{The medial tire graph for the tire in Figure~\ref{fig:tire-example}. The chord of $O$ is drawn faintly and omitted before taking the medial graph; medial edges between consecutive outer-boundary edges or consecutive inner-boundary edges are also omitted. Each medial vertex is placed at the midpoint of its corresponding retained tire edge.} \label{fig:medial-tire-example} \end{figure} \begin{theorem}[Annular medial colour bound] \label{thm:annular-medial-colour-bound} Let $T = (B_{\mathrm{out}}, O, E_{\mathrm{ann}})$ be a tire graph with non-degenerate boundaries and simple inner boundary $B_{\mathrm{in}}$. Let $A(T)$ be the subgraph of $M_{\mathrm{tire}}(T)$ induced by the annular medial vertices. For a graph $H$, write $\operatorname{Col}_3(H)$ for the set of proper $3$-vertex-colourings of $H$. Then $A(T)$ is a cycle and \[ |\operatorname{Col}_3(M_{\mathrm{tire}}(T))| \;\leq\; |\operatorname{Col}_3(A(T))|. \] \end{theorem} \begin{proof} Since the tread is a triangulated annulus with no vertices in its interior, each annular face has exactly one boundary edge, lying either on $B_{\mathrm{out}}$ or on $B_{\mathrm{in}}$, and exactly two annular edges. As the annular faces are traversed cyclically around the tread, consecutive faces share one annular edge. Equivalently, the annular edges occur in a cyclic order in which each annular face contains two consecutive annular edges. Hence the subgraph of $M_{\mathrm{tire}}(T)$ induced by the annular medial vertices is a cycle. Consider the restriction map from proper $3$-colourings of $M_{\mathrm{tire}}(T)$ to colourings of this annular medial cycle $A(T)$. We claim that this map is injective. Let $x$ be a non-annular medial vertex. Then $x$ corresponds to an edge of $B_{\mathrm{out}}$ or $B_{\mathrm{in}}$, since the chords of $O$ were omitted before forming $M_{\mathrm{tire}}(T)$. This boundary edge is incident to a unique annular face of $T^{\circ}$, and the other two edges of that face are annular edges. Therefore $x$ is adjacent in $M_{\mathrm{tire}}(T)$ to the two annular medial vertices corresponding to those two annular edges. Those two annular medial vertices are adjacent to each other, because their annular edges are consecutive on the same triangular annular face. In any proper $3$-colouring they therefore receive two distinct colours, and $x$ is forced to receive the remaining third colour. Thus every non-annular medial vertex has its colour uniquely determined by the colouring of $A(T)$. Two colourings of $M_{\mathrm{tire}}(T)$ with the same restriction to $A(T)$ are identical, so the restriction map is injective. The stated inequality follows. \end{proof} \begin{remark} \label{rem:tire-counts} Let $\mu = |V(B_{\mathrm{out}})|$ and $\nu = |V(B_{\mathrm{in}})|$. By Euler's formula on the tire tread $R$, the tire graph has $\mu + \nu$ triangular faces inside $R$ and $|E_{\mathrm{ann}}| = \mu + \nu$ annular edges when neither boundary is degenerate; when exactly one boundary is degenerate (so $\min(\mu, \nu) = 1$), there are $\mu + \nu - 1$ triangular faces and $|E_{\mathrm{ann}}| = \mu + \nu - 1$. \end{remark} \begin{proposition}[Source-side simple-cycle property] \label{prop:no-level-d-pinch} Let $G$ be a maximal planar graph with planar embedding $\Pi_G$ and single-vertex source $v_0$. Let $d \geq 1$, $v \in L_d$, and let $C'$ be a connected component of $G'_d$ such that $v$ is incident to some face in $F_{C'}$. Then the depth-$d$ faces in $F_{C'}$ incident to $v$ form a single contiguous arc in $v$'s rotation in $\Pi_G$. Equivalently: for any such component, the source-side boundary of $R_{C'}$ is a simple cycle in $L_d$ (no cut-vertices at level $d$). \end{proposition} \begin{proof} Suppose for contradiction that the depth-$d$ faces in $F_{C'}$ at $v$ lie in two or more disjoint arcs of $v$'s rotation. Adjacent vertices in $G$ differ in level by at most $1$, so a face at $v$ has depth exactly $d$ iff both other vertices have level $\geq d$, and depth $\leq d-1$ iff at least one has level $d-1$. Hence the gaps between the depth-$d$ arcs at $v$ are populated by level-$(d-1)$ neighbours of $v$, occurring in at least two disjoint arcs of $v$'s rotation. Pick $p$ in one such gap and $q$ in another. The BFS ball $G[L_{, blue!70!black, thin] (-2.5, -0.4) -- (-0.15, 0); \end{tikzpicture} \caption{Case 2 ($R$ = annulus) with $O$ a barbell. $B_{\mathrm{out}}$ is the outer hexagon (red); $O$ has two triangles $\{a_1, a_2, a_3\}$ and $\{b_1, b_2, b_3\}$ joined by the bridge $a_3\text{--}b_1$ (all light red). The annulus is triangulated by $14$ annular triangles: $6$ ``outer-cap'' triangles (one per outer edge), $6$ ``inner-cap'' triangles (one per non-bridge edge of $O$), and $2$ ``bridge-cap'' triangles $\{u_0, a_3, b_1\}$ and $\{u_3, a_3, b_1\}$ adjacent to the bridge. Each blue dot sits at the centroid of an annular triangle; blue edges connect dual vertices whose triangles share an interior annular edge (spoke or bridge). The two bridge-cap vertices have $\Gamma$-degree $3$ (their triangles have no boundary edge) and are joined by the dashed blue \emph{chord} corresponding to the bridge; the remaining $13$ edges form the Hamilton cycle that wraps around the annulus. All $14$ vertices lie on the outer face of the cycle-with-chord embedding, so $\Gamma \cong \Theta(1, 7, 7)$ is outerplanar.} \label{fig:inner-dual-annulus-case} \end{figure} \begin{remark} \label{rem:hamilton-cycle-spoke-only} In the \emph{spoke-only} case (Definition~\ref{def:tire-graph} with $O$ $2$-connected and $E_{\mathrm{ann}}$ consisting only of spokes), every annular face has exactly one boundary edge, every $d_f$ has $\Gamma$-degree $2$, and the construction of the Theorem~\ref{thm:inner-dual-outerplanar} proof reduces to the classical Hamilton cycle $\Gamma \cong C_{\mu+\nu}$ with zero chords. \end{remark} \begin{remark} \label{rem:bridge-case-theta} When $O$ has a bridge $e_{\mathrm{br}} \in E(O)$ whose two incident faces are annular triangles, $e_{\mathrm{br}}$ contributes an interior annular edge in $\Gamma$ rather than two leaves in $D(T)$ (see Definition~1.7 of \cite{bauerfeld-nested-tire-duals}). The two bridge-incident annular triangles have $\Gamma$-degree $3$; the resulting $\Gamma$ has the structure of a Hamilton cycle of length $\mu + \nu_\partial$ plus a single chord (length $1$). This corresponds to the theta graph $\Theta(1, b, c)$ identified empirically in \cite{bauerfeld-nested-tire-duals}, which has no $K_{2,3}$ subdivision (since one of the three paths has length $1$ and so contributes no degree-$2$ branch vertex), hence is outerplanar as predicted. \end{remark} \begin{theorem}[Tire treads form a rooted tree under face containment] \label{thm:tread-tree} Let $G$ be a maximal planar graph with planar embedding $\Pi_G$ and let $S \subseteq V(G)$ be a single-vertex level source $\{v_0\}$ lying on the outer face of $\Pi_G$. The collection $\mathcal{R}(G, S)$ of tire treads (Theorem~\ref{thm:tread-partition}) carries a canonical rooted tree structure $\mathcal{T}(G, S)$ defined as follows. \begin{itemize} \item \emph{Root.} The depth-$0$ tire tread $T_0$ --- the unique tire produced by Lemma~\ref{lem:tire-component} at $d = 0$, with degenerate outer boundary $B_{\mathrm{out}} = \{v_0\}$ and inner outerplanar graph $O^{(T_0)} = G[L_1]$ --- is the root. \item \emph{Parent.} For each tire tread $T_c$ at depth $d \ge 1$, its outer boundary $B_{\mathrm{out}}^{(T_c)}$ is a cycle in $L_d$. The \emph{parent} of $T_c$ is the unique tire tread $T_p$ at depth $d - 1$ whose inner outerplanar graph $O^{(T_p)}$ has $B_{\mathrm{out}}^{(T_c)}$ as the boundary cycle of one of its bounded faces. Equivalently, $R_c$ lies inside this bounded face of $O^{(T_p)}$ (which is itself the region of the plane cut off by $B_{\mathrm{out}}^{(T_c)}$ on the side away from $S$). \item \emph{Children.} The children of a tire tread $T_p$ are in bijection with those bounded faces of $O^{(T_p)}$ whose interiors contain at least one vertex of $G$ at level $\ge d + 2$ --- equivalently, with the connected components of $G'_{d+1}$ whose tires have outer boundary cycle equal to a bounded face of $O^{(T_p)}$. \end{itemize} Every tire tread except $T_0$ has exactly one parent; a tire tread may have zero, one, or several children. \end{theorem} \begin{proof} \emph{Root is well-defined.} At $d = 0$ with single-vertex source $S = \{v_0\}$, the dual subgraph $G'_0$ is connected (every face of $G$ incident to $v_0$ has dual depth $0$, and they form a single fan around $v_0$). By Lemma~\ref{lem:tire-component}, the unique component of $G'_0$ gives the depth-$0$ tire $T_0$ described above. \emph{Existence of parent.} Fix a tire tread $T_c$ at depth $d \ge 1$ arising from a connected component $C'_c$ of $G'_d$. Its outer boundary $B_{\mathrm{out}}^{(T_c)} = G[V_{C'_c} \cap L_d]$ is a simple cycle in $L_d$ (Lemma~\ref{lem:tire-component}; the source-side boundary of a tire is always a simple cycle, by Proposition~\ref{prop:no-level-d-pinch}). The faces of $G$ immediately outside $B_{\mathrm{out}}^{(T_c)}$ on the side facing $S$ have depth $d - 1$ (one of their three vertices lies in $L_{d-1}$, two in $L_d$). Let $C'_p$ be the connected component of $G'_{d-1}$ containing the dual vertex of any such face. \emph{Uniqueness of parent.} $B_{\mathrm{out}}^{(T_c)}$ is a single simple cycle in $G$, with a well-defined ``$S$-side'' (the side of the cycle closer to $v_0$ in $\Pi_G$). The depth-$(d-1)$ faces lying on this side form a single contiguous arc around $B_{\mathrm{out}}^{(T_c)}$ in the dual --- they are all $G'$-adjacent in sequence (each pair of consecutive arc faces shares an edge in $B_{\mathrm{out}}^{(T_c)}$). Hence they all lie in the same connected component $C'_p$ of $G'_{d-1}$, which is therefore unique. \emph{$B_{\mathrm{out}}^{(T_c)}$ bounds a face of $O^{(T_p)}$.} The parent tire $T_p$ has $V(O^{(T_p)}) = V_{C'_p} \cap L_d \supseteq V(B_{\mathrm{out}}^{(T_c)})$. The cycle $B_{\mathrm{out}}^{(T_c)}$ is a subgraph of $O^{(T_p)}$ that bounds a face of $O^{(T_p)}$ in the inherited embedding: the cycle traces around a depth-$\ge d+1$ region (containing $R_c$ and any descendants of $T_c$), which is exactly a bounded face of $O^{(T_p)}$. \emph{Children description.} The bounded faces of $O^{(T_p)}$ are in bijection with the connected components of $G'_d$ whose faces lie inside those bounded regions (= one component per bounded face, by an argument analogous to the existence-and- uniqueness step above, applied one level deeper). \emph{Tree property.} Every non-root $T_c$ has a unique parent at strictly smaller depth. Iterating the parent map strictly decreases depth, terminating at $T_0$. No cycles can form (depth is monotone). Hence $\mathcal{T}(G, S)$ is a rooted tree. \end{proof} \begin{remark} \label{rem:tree-multiple-children} A parent tire $T_p$ has multiple children precisely when its inner outerplanar graph $O^{(T_p)}$ has multiple bounded faces with non-trivial interiors (= containing depth-$\ge d+2$ vertices of $G$). This happens, for instance, when $O^{(T_p)}$ has chords or cut-vertices that subdivide its inner region. By contrast, if $O^{(T_p)}$ is a simple cycle (the spoke-only case of Remark~\ref{rem:hamilton-cycle-spoke-only}) with a non-empty interior, $T_p$ has exactly one child. \end{remark} \begin{theorem}[Tire-tree decomposition] \label{thm:tire-tree-decomposition} Let $G$ be a maximal planar graph with planar embedding $\Pi_G$ and let $v_0 \in V(G)$. The tree of tire treads $\mathcal{T}(G, \{v_0\})$ of Theorem~\ref{thm:tread-tree} \emph{decomposes $G$ into nested tires}: it is a finite rooted tree, rooted at the depth-$0$ tread containing $v_0$, whose nodes (tire treads) partition the bounded faces of $G$ (Theorem~\ref{thm:tread-partition}). This decomposition is moreover \emph{self-similar}. For any tread $T$ in $\mathcal{T}(G, \{v_0\})$ at depth $d \ge 1$, with outer-boundary cycle $C_T := B_{\mathrm{out}}^{(T)}$, let $G_T$ be the sub-graph of $G$ induced by $C_T$ together with all vertices of $G$ lying in the closed planar region $R_T \subset |\Pi_G|$ bounded by $C_T$ on the side of $C_T$ away from $v_0$. Then: \begin{enumerate} \item[(D1)] $G_T$, with the embedding inherited from $\Pi_G$, is a \emph{triangulated disk}: every bounded face is a triangle, and the outer face is bounded by $C_T$. \item[(D2)] Taking $C_T$ as a cycle source of $G_T$ (so $C_T$ has level $0$ in $G_T$ and the BFS-from-$C_T$ levels in $G_T$ equal $\ell_G(\cdot) - d$ on $V(G_T)$), the construction of Theorem~\ref{thm:tread-tree} extends to give a rooted tree of tire treads $\mathcal{T}(G_T, C_T)$ whose depth-$0$ root tread has $B_{\mathrm{out}} = C_T$ and inner outerplanar graph $O = O^{(T)}$. \item[(D3)] $\mathcal{T}(G_T, C_T)$ is canonically iso to the sub-tree of $\mathcal{T}(G, \{v_0\})$ rooted at $T$, preserving outer-boundary cycles, inner outerplanar graphs, and the parent--child face correspondence. \end{enumerate} In short: pick any vertex $v_0 \in V(G)$ to root the global tree $\mathcal{T}(G, \{v_0\})$ describing the whole graph; pick any tread $T$ in this tree; then $T$ is itself the root of a local tree $\mathcal{T}(G_T, C_T)$ describing the triangulated disk of $G$ inside $C_T$, with $C_T$ as cycle source. Maximal planar graphs decompose into nested trees of tire treads. \end{theorem} \begin{proof} \emph{Decomposition.} Theorem~\ref{thm:tread-tree} gives the rooted tree structure of $\mathcal{T}(G, \{v_0\})$, with root the depth-$0$ tread containing $v_0$; Theorem~\ref{thm:tread-partition} gives that its tire treads partition the bounded faces of $G$. Finiteness of the tree is immediate from finiteness of $G$. \emph{(D1) $G_T$ is a triangulated disk.} By Lemma~\ref{lem:tire-component} applied to the component of $G'_d$ that gives rise to $T$, the outer boundary $C_T = B_{\mathrm{out}}^{(T)}$ is a simple cycle in $L_d^G$. By the Jordan curve theorem, $C_T$ separates $|\Pi_G| \setminus C_T$ into two open regions; $R_T$ is the closure of the one not containing $v_0$. The bounded faces of $G_T$ in its inherited embedding are exactly the bounded faces of $G$ contained in $R_T$, each of which is a triangle since $G$ is a triangulation. The unbounded face of $G_T$'s embedding is the complement of $R_T$, whose boundary is $C_T$. \emph{(D2) Level shift.} We show $\mathrm{dist}_{G_T}(v, C_T) = \ell_G(v) - d$ for every $v \in V(G_T)$. When $v \in C_T$ both sides equal $0$, so fix $v \in V(G_T) \setminus C_T$. \smallskip \emph{Step 1: $\mathrm{dist}_G(v, C_T) = \ell_G(v) - d$.} A shortest $G$-path from $v$ to $v_0$ must visit $C_T$, since $v$ and $v_0$ lie in different open regions of $|\Pi_G| \setminus C_T$; let $w$ be its first $C_T$-vertex. The $v$-to-$w$ sub-path has length $\ge \mathrm{dist}_G(v, C_T)$ and the $w$-to-$v_0$ sub-path has length $\ell_G(w) = d$, so $\ell_G(v) \ge \mathrm{dist}_G(v, C_T) + d$. Conversely, concatenating a shortest $G$-path from $v$ to a nearest $C_T$-vertex $w'$ with a shortest $G$-path from $w'$ to $v_0$ gives a $v$-to-$v_0$ path of length $\mathrm{dist}_G(v, C_T) + d$, so $\ell_G(v) \le \mathrm{dist}_G(v, C_T) + d$. \smallskip \emph{Step 2: $\mathrm{dist}_{G_T}(v, C_T) = \mathrm{dist}_G(v, C_T)$.} The inequality $\ge$ is automatic since $G_T \subseteq G$. For $\le$, pick a shortest $G$-path $\pi$ from $v$ to $C_T$; we may assume $\pi$ has no internal vertex in $C_T$ (truncate otherwise). Any internal vertex of $\pi$ then lies in the same open region of $|\Pi_G| \setminus C_T$ as $v$, i.e.\ in $R_T \setminus C_T \subseteq V(G_T)$; every edge of $\pi$ has both endpoints in $V(G_T)$ and so lies in $E(G_T)$. Hence $\pi$ is a path in $G_T$ realising $\mathrm{dist}_G(v, C_T)$. \smallskip Combining the two steps yields $\mathrm{dist}_{G_T}(v, C_T) = \ell_G(v) - d$, as claimed. \emph{(D3) Tree iso.} By (D2), $L_k^{G_T} = L_{d+k}^G \cap V(G_T)$ for every $k \ge 0$. For a bounded face $f$ of $G_T$, dual depth in $G_T$ equals $\min_{u \in V(f)} \ell_{G_T}(u) = \min_{u \in V(f)} \ell_G(u) - d = \delta_G(d_f) - d$. Hence the inner-dual subgraph $(G_T)'_{k}$ at depth $k$ in $G_T$ is the induced subgraph of $G'_{d+k}$ on the faces of $G$ lying in $R_T$, and two such faces are dual-adjacent in $G_T'$ iff they are dual-adjacent in $G'$ (the shared edge is in $E(G_T)$). \smallskip \emph{Step 3: components of $(G_T)'_{k}$ are precisely the depth-$(d+k)$ descendants of $T$ in $\mathcal{T}(G, \{v_0\})$.} We show by induction on $k$ that a component $C'$ of $G'_{d+k}$ has $F_{C'} \subseteq R_T$ iff $C'$ is a depth-$(d+k)$ descendant of $T$. For $k = 0$: the components of $G'_d$ are the depth-$d$ treads; the component giving rise to $T$ has its faces in $T$'s tread region $R \subseteq R_T$, while any other depth-$d$ tread $T''$ has $C_{T''}$ disjoint from $C_T$ and lying in a different bounded face of $O^{(T_p'')}$ at depth $d - 1$, hence $R_{T''} \cap R_T = \emptyset$. For $k \ge 1$: by Theorem~\ref{thm:tread-tree}, each component $C'$ of $G'_{d+k}$ has a unique parent $C'_p$ at depth $d+k-1$, with $B_{\mathrm{out}}^{(C')}$ bounding a face of $O^{(C'_p)}$; equivalently $R_{C'}$ lies inside that bounded face, hence inside $R_{C'_p}$. By the induction hypothesis $R_{C'_p} \subseteq R_T$ iff $C'_p$ is a descendant of $T$ at depth $d+k-1$, and $R_{C'} \subseteq R_{C'_p}$, so $R_{C'} \subseteq R_T$ iff $C'$ is a descendant of $T$ at depth $d+k$. \smallskip \emph{Step 4: tread data and child--face correspondence.} The Tire-component lemma (Lemma~\ref{lem:tire-component}) and the source-side simple-cycle property (Proposition~\ref{prop:no-level-d-pinch}) extend verbatim to the cycle-sourced triangulated disk $(G_T, C_T)$: the proofs use only the triangular structure of bounded faces, the local arrangement of faces around each vertex's rotation, and the connectivity of the BFS ball $G_T[L_{